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Slide 1
Slide 1

... Noble Gases are colorless gases that are extremely unreactive. One important property of the noble gases is their inactivity. They are inactive because their outermost energy level is full. Because they do not readily combine with other elements to form compounds, the noble gases are called inert. T ...
ESCI110,FinalPract,Ex,F07
ESCI110,FinalPract,Ex,F07

... A) sinking of oceanic lithosphere into the mantle at a subduction zone B) transform faulting between an oceanic plate and a continental plate C) rifting beneath a continental plate and the beginning of continental drift D) rising of hot asthenosphere from deep in the mantle 61) When an earthquake oc ...
Sea-Floor Spreading - Madison County Schools
Sea-Floor Spreading - Madison County Schools

... • Using a submarine named Alvin, scientists were able to look into a rift valley and examine something called pillow lava, which is a special type of solid rock that only forms on the ocean floor when magma cools very rapidly. This proved that new molten material was being added to the ocean floor a ...
4.2 The Theory of Plate Tectonics
4.2 The Theory of Plate Tectonics

... Tectonics: The study of the formation of features in the earth’s crust Open textbook to p. 72 ...
C1 Revision Checklist
C1 Revision Checklist

... c) Convection currents within the Earth’s mantle driven by heat released by natural radioactive processes cause the plates to move at relative speeds of a few centimetres per year. d) The movements can be sudden and disastrous. Earthquakes and / or volcanic eruptions occur at the boundaries between ...
The sea floor spreads apart at divergent boundaries.
The sea floor spreads apart at divergent boundaries.

... The sea floor spreads apart at divergent boundaries. In the ocean, divergent boundaries are also called spreading centers. Mid-ocean ridges mark these sites where the ocean floor is spreading apart. As the ridges continue to widen, a gap called a rift valley forms. Here molten material rises to buil ...
THE EXAM WILL INCLUDE TH FOLLOWING QUESTIONS PART A
THE EXAM WILL INCLUDE TH FOLLOWING QUESTIONS PART A

... Composition Texture ...
LECTURE W3-L7-9 - Partial Melting
LECTURE W3-L7-9 - Partial Melting

... decompression melting of the rising asthenosphere, results in bimodal postorogenic magmatism with both mafic mantle and silicic crustal melts. Winter (2001) An Introduction to Igneous and Metamorphic Petrology. ...
Higher Tier, Unit C2: Chemistry
Higher Tier, Unit C2: Chemistry

Plate Tectonics
Plate Tectonics

... The Wilson Cycle ...
Chapter 33
Chapter 33

... – Forms a deep ocean trench – Crust deep in trench melts, produces magma which can lead to volcanic island arcs ...
MYSTERIES OF PLANET EARTH
MYSTERIES OF PLANET EARTH

... Mass; Pressure >3 Million atmosph.; Temp.~4,700ºC; Composition: IRON-NICKEL, Consistent with Seismic data, meteorite data, and mathematical model ...
Tectonic Plates
Tectonic Plates

... 14-3 What Are Mineral Resources, and what are their Environmental Effects?  Concept 14-3A Some naturally occurring materials in the earth’s crust can be extracted and made into useful products in processes that provide economic benefits and jobs.  Concept 14-3B Extracting and using mineral resour ...
File
File

... Geological Processes and how they shape our Earth There are many different types of geological processes some slow, and some fast. They are constantly at work changing the face of our earth, both destroying land, and creating new land. ...
Inside the Earth
Inside the Earth

... made of basalt) – Continental (less dense, made of granite) ...
Sea-Floor Spreading
Sea-Floor Spreading

... of a long system of mountains that winds beneath Earth’s oceans.  Ex. East Pacific Rise  Sonar: a device that bounces sound waves off underwater objects and then records the echoes of these sound waves.  Scientists used this to map the ocean floor.  The time it takes for the echo to arrive indic ...
Chapter 7, Section 1 - Answer Key
Chapter 7, Section 1 - Answer Key

... while the densest compounds make up the core? Heavier elements are pulled to the center of the Earth by gravity. The elements with less mass are further from the center. 4. List the three layers of the Earth, based on their chemical composition. Crust, mantle, core (outer and inner) 5. Complete Sent ...
Volcanoes-Earthquakes
Volcanoes-Earthquakes

... The plates, which make up Earth's lithosphere, float on a semi-solid layer of molten rock called the mantle or the asthenosphere. The mantle has two layers: (1) the upper mantle which is more solid and (2) the lower mantle which is more liquid. ...
Emplacement mechanism of the Middle
Emplacement mechanism of the Middle

... 2) the contact between the granite and country rocks is sharp, with a 1-10m narrow thermal aureole, but without any visible deformation. The microscopic observation on the thin sections of wall rocks and granite doesn’t show any mineral preferred orientation consisting to the field observation. Ther ...
Ch. 9 Review - 8th Grade Science
Ch. 9 Review - 8th Grade Science

The Earth Handbook
The Earth Handbook

August 2008
August 2008

... Which rock is formed when a layer of shale becomes metamorphosed? (A) (B) (C) (D) ...
Unit Name: Earth`s History - Red Clay Secondary Science Wiki
Unit Name: Earth`s History - Red Clay Secondary Science Wiki

... 7.2.A. The Earth’s present day species evolved from earlier, distinctly different species. Many thousands of layers of sedimentary rock provide evidence for the long history of the Earth and for the long history of changing life forms whose remains are found in the rocks. More recently deposited roc ...
No Slide Title
No Slide Title

... When an ocean plate and continental plate collide, this plate will subduct because it is denser ...
The Mantle
The Mantle

... and pressures so great that the metals are squeezed together and are not able to move.  Therefore; the inner core is a solid.  The temperature in the core is nearly as hot as the surface of the SUN! ...
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Geochemistry

Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt.
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